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The Geological Characteristics for Pre-Cambrian Shale Gas Accumulation in China

机译:中国前寒武纪页岩气累积的地质特征

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摘要

China has huge shale gas resources potential. The exploitation of shale gas can effectively reduce atmosphere pollution and relieve the energy shortage in China. Organic rich shale in pre-Cambrian period mainly lies to North China and Yangtze areas. The shales were developed in continental shelf and restricted marine basin. The distribution is stable with the thickness ranging from 10m-150m. The geochemistry characteristics are favored for shale gas accumulation for pre-Cambrian shale. The shale mineral is mainly quartz and feldspar. The pre-Cambrian formations have favored geological condition for shale gas accumulation. The favored intervals and regions for development of shale gas are Doushantuo shale in Upper Yangtze areas and Hongshuizhuang shale in northern Hebei Province or Jianchang Basin in western Liaoning Province.
机译:中国有巨大的页岩气资源潜力。页岩气的开采可以有效地减少大气污染,减轻了中国的能源短缺。寒武纪前期有机丰富的页岩主要位于华北地区和长江地区。 Shales是在大陆架和限制的海滨盆地开发的。该分布稳定,厚度范围为10m-150m。地球化学特征对寒武纪页岩的页岩气累积有利于。页岩矿物主要是石英和长石。寒武纪前的形成对页岩气累积的地质条件有利。页岩气发展的青睐间隔和地区是河北省北部冬月地区的Doushantuo页岩,在辽西省的建昌盆地。

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